In common usage, wind gradient, more specifically wind speed gradient or wind velocity gradient, or alternatively shear wind, is the vertical component... 35 KB (4,299 words) - 16:29, 29 February 2024 |
Speed of sound (section Effects due to wind shear) the source. Wind shear of 4 m/(s · km) can produce refraction equal to a typical temperature lapse rate of 7.5 °C/km. Higher values of wind gradient will... 56 KB (7,925 words) - 02:25, 23 April 2024 |
consumption. Areas of wind shear caused by various weather phenomena can lead to dangerous situations for aircraft. When winds become strong, trees and... 105 KB (11,196 words) - 02:32, 23 April 2024 |
Tropical cyclone (redirect from Tropical cyclone wind speed climatology) Atlantic (although occasional examples do occur) due to consistently strong wind shear and a weak Intertropical Convergence Zone. In contrast, the African easterly... 211 KB (20,725 words) - 03:22, 14 May 2024 |
Squall line (section Wind shear) behind the line will produce a mesohigh. Wind shear is an important aspect of a squall line. In low to medium shear environments, mature thunderstorms will... 14 KB (1,641 words) - 20:23, 13 February 2024 |
thunderstorms move with the mean wind flow through the layer of the troposphere that they occupy, vertical wind shear sometimes causes a deviation in their... 80 KB (8,542 words) - 00:51, 10 May 2024 |
Wind shear is a difference in wind speed and direction over a relatively short distance in the atmosphere. It may also refer to: Windshear (comics), a... 370 bytes (80 words) - 07:23, 15 October 2015 |
Squall (redirect from Barat (wind)) damaging) winds. Wind shear is an important aspect to measuring the potential of squall line severity and duration. In low to medium shear environments... 16 KB (1,931 words) - 03:32, 27 December 2023 |